Transverse wave
A transverse wave is formed when particles move forward at the crest and backward at the trough. In a transverse wave, the particles oscillate perpendicular to the direction of wave propagation. Examples of transverse waves include electromagnetic waves and waves on a string.
rarefaction is equivalent to trough and compression is equivalnet to crest
The region of spread out particles in a wave is called the trough. This is where the particles are at their lowest point of displacement from their equilibrium position.
trough.
This type of wave is called a plunging wave. Plunging waves are characterized by a curling crest that falls forward and crashes into the trough with a lot of energy, making them popular with surfers.
A transverse wave is formed when particles move forward at the crest and backward at the trough. In a transverse wave, the particles oscillate perpendicular to the direction of wave propagation. Examples of transverse waves include electromagnetic waves and waves on a string.
rarefaction is equivalent to trough and compression is equivalnet to crest
The region of spread out particles in a wave is called the trough. This is where the particles are at their lowest point of displacement from their equilibrium position.
trough.
This type of wave is called a plunging wave. Plunging waves are characterized by a curling crest that falls forward and crashes into the trough with a lot of energy, making them popular with surfers.
No, the height of a wave's trough is not directly dependent on its amplitude. The amplitude of a wave is the maximum displacement of particles from their rest position, while the height of the wave's trough is determined by the distance from the crest to the trough. These two aspects of a wave are related but not directly proportional.
In a transverse wave, the trough represents the lowest point where the displacement of the wave is at its minimum value. This is because the trough corresponds to the region of the wave where the particles are at their lowest point of oscillation, moving in opposite direction to the direction of wave propagation.
An aulacogen is a tectonic trough on a craton which is formed as the failed arm of a triple-rift junction.
A naturally formed sloped and sided trough where streams flow or have flowed in the past.
In a compressional wave, the particles are spaced farthest apart at the points of maximum rarefaction where the wave is at its trough. This is when the pressure is at its lowest and the particles are more spread out.
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Trough